Abstract
The paper presents an autosoliton model of slow deformation perturbations propagating in the elements of the Earth’s crust. The model describes well both the migration of seismic activations (running autosolitons) and the formation of fault zones (static and pulsating autosolitons). When two autosolitons meet, they interact as not completely elastic particles, their amplitudes and shapes noticeably change.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
